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Science Q-1
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Cards (43)
Lithosphere
The rocky skin of
Earth
Essential learning competency
Describe and relate the distribution of active volcanoes, earthquake epicenters, and major mountain belts to plate tectonic fury
Objectives
Describe the Earth's
lithosphere
Differentiate
oceanic
and
continental
crust
Infer that the
Earth's
lithosphere is divided into
plates
Identify the major
lithospheric
plates
Determine the
scientific
basis for dividing the
lithospheric
plates
The world map shows
countries
, continents,
oceans
, and islands
Tectonic plates
Smaller
sections of the
lithosphere
Plate boundaries
Edges that
separate
the
tectonic plates
Types of lithospheric plates
Continental
lithosphere
Oceanic
lithosphere
Continental lithosphere
Thick, found under land masses, average thickness of
25-70
km, composed of old rocks, average density of 2.7 g/cm^3, mostly made of
granite
Oceanic lithosphere
Thinner, younger, denser with average density of 3.0 g/cm^3, mostly made of
basalt
Types of plates
Primary
plates
Secondary
plates
Primary plates
Larger
plates
Secondary plates
Smaller
plates
Primary plates
Pacific
plate
North American
plate
Eurasian
plate
African
plate
Antarctic
plate
Australian
plate
South American
plate
Secondary plates
Juan de Fuca
plate
Nazca
plate
Cocos
plate
Caribbean
plate
Philippine
plate
Arabian
plate
Indian
plate
Scotia
plate
Basis for dividing lithospheric plates
1.
Gathering data
on
earthquake epicenters
2.
Mapping volcanic activities
3.
Identifying major mountain ranges
Earthquake
epicenters, volcanic activities, and major mountain ranges
Distributed
near
or
along
plate boundaries
Scientists
use these geologic
events and features to identify and plot plate boundaries
Epicenter
Location on the
surface
of the earth directly above the
focus
Focus
Point within the earth where
energy
is released
The epicenter of the earthquake in the article is in
Balayan Bay
,
Batangas City
Magnitude
Number that characterizes the relative size of an earthquake, the
higher
the number the
stronger
the earthquake
The magnitude of the earthquake in the article is
5.4
, which is
moderate
Seismic waves
Energy released from an earthquake, recorded by
seismographs
, generated by the movement of
tectonic plates
Types of seismic waves
Body waves
Surface waves
Body waves
Travel into the
interior
of the earth
Surface waves
Travel through the crust, do not travel into the
interior
of the earth
waves (Primary waves)
Fastest
seismic
waves, longitudinal, can move through
solid rock
and fluids
waves (Secondary waves)
Slower
than P-waves, transverse, can only move through
solids
Love waves
Most
damaging
type of
surface wave
, named after British mathematician Augustus Edward H. Love
Rayleigh waves
Cause most of the shaking felt during an
earthquake
, named after scientist Lord Rayleigh (
John William Strutt
)
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